No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70260863","usgsCitation":"U.S. Geological Survey, 1978, Hydrologic unit map - 1978, State of California, https://doi.org/10.3133/70260863.","costCenters":[],"links":[{"id":463888,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Barker, James L.","contributorId":53000,"corporation":false,"usgs":true,"family":"Barker","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":829286,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70233091,"text":"70233091 - 1978 - Galiuro Volcanics, Pinal, Graham, and Cochise counties, Arizona","interactions":[],"lastModifiedDate":"2022-07-15T16:57:02.931314","indexId":"70233091","displayToPublicDate":"1978-01-01T11:52:09","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Galiuro Volcanics, Pinal, Graham, and Cochise counties, Arizona","docAbstract":"The Galiuro Volcanics occurs in the Galiuro, Winchester, and Little Dragoon Mountains, east and northeast of Tucson, Ariz. The sequence comprises lava flows and ash-flow tuffs ranging in composition from andesite to rhyolite. In general they can be subdivided into two parts separated by a major erosional unconformity. The lower part is predominantly lava flows ranging from andesite to rhyodacite but contains three ash-flow tuffs. The upper part is chiefly ash-flow tuff but also includes two areas of rhyolite-obsidian flows and domes and rhyolitic to andesitic flows. Conglomerate separates many if not all of the rock units in the upper part. The individual flows and tuffs are lenticular, and the stratigraphic relations are complex. Chemical variation diagrams suggest consanguinity among all the volcanic rocks, but the complex intercalation of rhyolite and andesite and of lava flows and ash-flow tuff indicates more than one magma chamber, different stages of differentiation in separate magma chambers, and several eruption centers. Chemical analyses indicate that the magmas were normal calc-alkaline. Eleven potassium-argon age determinations indicate that the Galiuro Volcanics accumulated from about 29 to 23 million years ago, which is in the middle of the mid-Tertiary volcanic and plutonic event in Arizona.
","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Creasey, S., and Krieger, M.H., 1978, Galiuro Volcanics, Pinal, Graham, and Cochise counties, Arizona: Journal of Research of the U.S. Geological Survey, v. 6, no. 1, p. 115-131.","productDescription":"17 p.","startPage":"115","endPage":"131","costCenters":[],"links":[{"id":403838,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403837,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Cochise County, Graham County, Pinal County","otherGeospatial":"Galiuro Volcanics","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.77490234375,\n 31.287939892641734\n ],\n [\n -109.720458984375,\n 31.287939892641734\n ],\n [\n -109.720458984375,\n 33.04550781490999\n ],\n [\n -111.77490234375,\n 33.04550781490999\n ],\n [\n -111.77490234375,\n 31.287939892641734\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Creasey, S.C.","contributorId":36109,"corporation":false,"usgs":true,"family":"Creasey","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":846699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krieger, Medora H.","contributorId":62188,"corporation":false,"usgs":true,"family":"Krieger","given":"Medora","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":846700,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":33171,"text":"b1457 - 1978 - Contributions to stratigraphy","interactions":[{"subject":{"id":47424,"text":"b1457A - 1978 - Changes in stratigraphic nomenclature by the U. S. Geological Survey, 1977","indexId":"b1457A","publicationYear":"1978","noYear":false,"chapter":"A","title":"Changes in stratigraphic nomenclature by the U. S. Geological Survey, 1977"},"predicate":"IS_PART_OF","object":{"id":33171,"text":"b1457 - 1978 - Contributions to stratigraphy","indexId":"b1457","publicationYear":"1978","noYear":false,"title":"Contributions to stratigraphy"},"id":1},{"subject":{"id":47425,"text":"b1457B - 1979 - Stratigraphy and depositional environment of the Dutch Harbor Member of the Unalaska Formation, Unalaska Island, Alaska","indexId":"b1457B","publicationYear":"1979","noYear":false,"chapter":"B","title":"Stratigraphy and depositional environment of the Dutch Harbor Member of the Unalaska Formation, Unalaska Island, Alaska"},"predicate":"IS_PART_OF","object":{"id":33171,"text":"b1457 - 1978 - Contributions to stratigraphy","indexId":"b1457","publicationYear":"1978","noYear":false,"title":"Contributions to stratigraphy"},"id":2},{"subject":{"id":47426,"text":"b1457C - 1979 - The Holocene Ridgeland Formation and associated Decker Soil (new names) near Great Salt Lake, Utah","indexId":"b1457C","publicationYear":"1979","noYear":false,"chapter":"C","title":"The Holocene Ridgeland Formation and associated Decker Soil (new names) near Great Salt Lake, Utah"},"predicate":"IS_PART_OF","object":{"id":33171,"text":"b1457 - 1978 - Contributions to stratigraphy","indexId":"b1457","publicationYear":"1978","noYear":false,"title":"Contributions to stratigraphy"},"id":3},{"subject":{"id":47427,"text":"b1457D - 1978 - Abandonment of the name Hartford Hill Rhyolite Tuff and adoption of new formation names for middle Tertiary ash-flow tuffs in the Carson City-Silver City area, Nevada","indexId":"b1457D","publicationYear":"1978","noYear":false,"chapter":"D","title":"Abandonment of the name Hartford Hill Rhyolite Tuff and adoption of new formation names for middle Tertiary ash-flow tuffs in the Carson City-Silver City area, Nevada"},"predicate":"IS_PART_OF","object":{"id":33171,"text":"b1457 - 1978 - Contributions to stratigraphy","indexId":"b1457","publicationYear":"1978","noYear":false,"title":"Contributions to stratigraphy"},"id":4},{"subject":{"id":47428,"text":"b1457E - 1979 - Stratigraphic nomenclature of the central Santa Monica Mountains, Los Angeles County, California, with a section on Age of the Conejo Volcanics","indexId":"b1457E","publicationYear":"1979","noYear":false,"chapter":"E","title":"Stratigraphic nomenclature of the central Santa Monica Mountains, Los Angeles County, California, with a section on Age of the Conejo Volcanics"},"predicate":"IS_PART_OF","object":{"id":33171,"text":"b1457 - 1978 - Contributions to stratigraphy","indexId":"b1457","publicationYear":"1978","noYear":false,"title":"Contributions to stratigraphy"},"id":5},{"subject":{"id":47429,"text":"b1457F - 1978 - Stratigraphic revision of the middle Eocene, Oligocene, and lower Miocene; Atlantic Coastal Plain of North Carolina","indexId":"b1457F","publicationYear":"1978","noYear":false,"chapter":"F","title":"Stratigraphic revision of the middle Eocene, Oligocene, and lower Miocene; Atlantic Coastal Plain of North Carolina"},"predicate":"IS_PART_OF","object":{"id":33171,"text":"b1457 - 1978 - Contributions to stratigraphy","indexId":"b1457","publicationYear":"1978","noYear":false,"title":"Contributions to stratigraphy"},"id":6},{"subject":{"id":47430,"text":"b1457G - 1979 - Revisions in stratigraphic nomenclature of the Columbia River Basalt Group","indexId":"b1457G","publicationYear":"1979","noYear":false,"chapter":"G","title":"Revisions in stratigraphic nomenclature of the Columbia River Basalt Group"},"predicate":"IS_PART_OF","object":{"id":33171,"text":"b1457 - 1978 - Contributions to stratigraphy","indexId":"b1457","publicationYear":"1978","noYear":false,"title":"Contributions to stratigraphy"},"id":7}],"lastModifiedDate":"2014-06-30T11:45:29","indexId":"b1457","displayToPublicDate":"1978-01-01T11:43:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1457","title":"Contributions to stratigraphy","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1457","usgsCitation":"U.S. Government Printing Office, 1978, Contributions to stratigraphy: U.S. Geological Survey Bulletin 1457, 7 v., https://doi.org/10.3133/b1457.","productDescription":"7 v.","costCenters":[],"links":[{"id":289201,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53b286e6e4b07b8813a5547a"} ,{"id":70233086,"text":"70233086 - 1978 - Implications of the petrochemistry of palladium at Iron Canyon, Lander County, Nevada","interactions":[],"lastModifiedDate":"2022-07-15T16:51:02.914651","indexId":"70233086","displayToPublicDate":"1978-01-01T11:42:30","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Implications of the petrochemistry of palladium at Iron Canyon, Lander County, Nevada","docAbstract":"Approximately one-half of the 270 samples from the Iron Canyon area, Nevada, analyzed for platinum-group metals, contain measurable amounts of palladium in the 0.001- to 0.02-part per million range with an average of 0.0034 ppm. The rocks include lower Paleozoic sedimentary and volcanic rocks, Tertiary granitic porphyries, and breccia, all of which exhibit various degrees of hydrothermal alteration. Fault-related iron oxides and vein quartz are also present. The area lies astride the outermost fringes of the zone of dispersed alteration visible in outcrops around the middle Tertiary porphyry-copper system at Copper Canyon, Nevada. At Iron Canyon, the palladium concentrations greater than 0.003 ppm seem to be spatially related to the Butte fault zone, a north-striking fault system active during the time of porphyry-type mineralization. Palladium contents vary directly with those of mercury, arsenic, strontium, silver, lanthanum, and boron, as well as with lead, gold, and copper in obviously metallized rocks. This relation probably reflects the mobility of palladium during porphyry-type mineralization. However, our study failed to document conclusively the overall introduction of palladium during mineralization. Among the likely sources of palladium are the lower Paleozoic volcanic rocks or fluids equilibrated with magma (s) associated with the middle Tertiary porphyries.
","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Page, N.J., and Theodore, T., 1978, Implications of the petrochemistry of palladium at Iron Canyon, Lander County, Nevada: Journal of Research of the U.S. Geological Survey, v. 6, no. 1, p. 107-114.","productDescription":"8 p.","startPage":"107","endPage":"114","costCenters":[],"links":[{"id":403836,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403834,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","county":"Lander County","otherGeospatial":"Iron Canyon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.26257324218749,\n 40.500225211369\n ],\n [\n -117.01812744140625,\n 40.500225211369\n ],\n [\n -117.01812744140625,\n 40.70875101828792\n ],\n [\n -117.26257324218749,\n 40.70875101828792\n ],\n [\n -117.26257324218749,\n 40.500225211369\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Page, Norman J.","contributorId":46492,"corporation":false,"usgs":true,"family":"Page","given":"Norman","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":846697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Theodore, Ted G.","contributorId":57840,"corporation":false,"usgs":true,"family":"Theodore","given":"Ted G.","affiliations":[],"preferred":false,"id":846698,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70119884,"text":"70119884 - 1978 - Landsat digital data classification for land use and wildlife habitat inventory","interactions":[],"lastModifiedDate":"2014-08-11T11:36:57","indexId":"70119884","displayToPublicDate":"1978-01-01T11:36:20","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Landsat digital data classification for land use and wildlife habitat inventory","docAbstract":"No abstract available.","language":"English","publisher":"Bendix Aerospace Systems Division","publisherLocation":"Ann Arbor, MI","usgsCitation":"Bendix Aerospace Systems Division, 1978, Landsat digital data classification for land use and wildlife habitat inventory.","costCenters":[],"links":[{"id":291954,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e9d8d3e4b008eaa4f3f667"} ,{"id":70039404,"text":"70039404 - 1978 - The United States Geological Survey","interactions":[],"lastModifiedDate":"2012-08-04T01:01:57","indexId":"70039404","displayToPublicDate":"1978-01-01T11:34:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"The United States Geological Survey","docAbstract":"The Geological Survey is a Federal research and fact-finding agency that provides for the people of the United States","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039404","usgsCitation":"United States Geological Survey, 1978, The United States Geological Survey: General Information Product, 27 p., https://doi.org/10.3133/70039404.","productDescription":"27 p.","numberOfPages":"28","costCenters":[],"links":[{"id":261554,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039404/report.pdf"},{"id":261555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039404/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba95de4b08c986b322204","contributors":{"authors":[{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":535292,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70233085,"text":"70233085 - 1978 - Igneous and metamorphic petrology of the southwestern Dana Mountains, Lassiter Coast, Antarctic Peninsula","interactions":[],"lastModifiedDate":"2022-07-15T16:40:52.671559","indexId":"70233085","displayToPublicDate":"1978-01-01T11:31:17","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Igneous and metamorphic petrology of the southwestern Dana Mountains, Lassiter Coast, Antarctic Peninsula","docAbstract":"The southwestern Dana Mountains of the southern Antarctic Peninsula are underlain by the western part of a composite concentrically zoned Upper Cretaceous batholith consisting largely of granodiorite. The granodiorite (felsic phase) was intrusive into older heterogeneous gabbro-diorite (mafic phase) which makes up the margin of the batholith. Flat-lying pegmatite bodies and abundant inclusions, roof pendants, and septa of metasedimentary rocks and gabbrodiorite suggest that the granodiorite lies near the roof of the batholith. Petrography, chemistry, field relations, and radiometric age dates indicate that the batholith is part of the Andean intrusive suite, a suite of calc-alkaline plutonic rocks that crops out extensively throughout the Antarctic Peninsula and Chilean and Patagonian Andes. Textural features, mineralogy, and chemical data indicate that both phases of the batholith in the southwestern Dana Mountains have been contaminated by assimilation of the Latady Formation, an Upper Jurassic sequence of shale, siltstone, and sandstone that underlies large parts of the southern Antarctic Peninsula. Composition of the granodiorite also has been modified by assimilation of lesser amounts of the gabbro-diorite phase. Such contaminated plutonic rocks occur in several places in the northern Antarctic Peninsula; the batholith in the southwestern Dana Mountains represents the southernmost exposures of contaminated igneous rocks known from the Antarctic Peninsula. Hornblende andesite dikes cut both the mafic and felsic phases of the batholith. Chemical data imply that the dikes represent small amounts of mafic material remobilized by intrusion of the granodiorite. During the austral summers of 1969
","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Vennum, W.R., 1978, Igneous and metamorphic petrology of the southwestern Dana Mountains, Lassiter Coast, Antarctic Peninsula: Journal of Research of the U.S. Geological Survey, v. 6, no. 1, p. 95-106.","productDescription":"12 p.","startPage":"95","endPage":"106","costCenters":[],"links":[{"id":403832,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403830,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Antarctica","otherGeospatial":"Antarctic Peninsula, Dana Mountains, Lassiter Coast","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -65,\n -74\n ],\n [\n -61,\n -74\n ],\n [\n -61,\n -72.5\n ],\n [\n -65,\n -72.5\n ],\n [\n -65,\n -74\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Vennum, Walter R.","contributorId":146859,"corporation":false,"usgs":false,"family":"Vennum","given":"Walter","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":846695,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70233079,"text":"70233079 - 1978 - Petrology of the Precambrian intrusive center at Lake George, southern Front Range, Colorado","interactions":[],"lastModifiedDate":"2022-07-15T16:30:21.681979","indexId":"70233079","displayToPublicDate":"1978-01-01T11:25:32","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Petrology of the Precambrian intrusive center at Lake George, southern Front Range, Colorado","docAbstract":"The intrusive center at Lake George, at the western margin of the Pikes Peak batholith (1030 m.y.) of central Colorado, contains rocks of both the potassic and sodic differentiation trends recognized in the batholith. Finer grained variants of the Pikes Peak Granite initially formed a texturally zoned stock 8 kilometers in diameter that cut the dominant coarse-grained granite of the batholith. This granite stock (potassic trend) was later intruded by partial ring dikes of quartz syenite to fayalite granite and by a central stock of quartz syenite to syenomonzonite (sodic trend). Xenoliths of alkali gabbro, diorite porphyry, and granodiorite are included within rocks of both differentiation trends. All major rock types of the intrusive center are thought to be derivatives of alkali basaltic magma from the mantle, modified by fractional crystallization and reaction melting of crustal rocks. The geometry of the intrusive center was controlled by ring-dike/cauldron-subsidence mechanisms.
","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Wobus, R.A., and Anderson, R.S., 1978, Petrology of the Precambrian intrusive center at Lake George, southern Front Range, Colorado: Journal of Research of the U.S. Geological Survey, v. 6, no. 1, p. 81-94.","productDescription":"14 p.","startPage":"81","endPage":"94","costCenters":[],"links":[{"id":403826,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403825,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Front Range, Lake George","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.64041137695312,\n 38.78941577989049\n ],\n [\n -104.81231689453125,\n 38.78941577989049\n ],\n [\n -104.81231689453125,\n 39.386325215154336\n ],\n [\n -105.64041137695312,\n 39.386325215154336\n ],\n [\n -105.64041137695312,\n 38.78941577989049\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wobus, R. A.","contributorId":70745,"corporation":false,"usgs":true,"family":"Wobus","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":846689,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, R. S.","contributorId":255428,"corporation":false,"usgs":false,"family":"Anderson","given":"R.","email":"","middleInitial":"S.","affiliations":[{"id":12698,"text":"Northern Arizona University","active":true,"usgs":false}],"preferred":false,"id":846690,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70119881,"text":"70119881 - 1978 - Outline for the characterization of and impact assessment for the aquatic systems of the Wyoming-Montana coal test area","interactions":[],"lastModifiedDate":"2014-08-11T11:19:01","indexId":"70119881","displayToPublicDate":"1978-01-01T11:16:48","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Outline for the characterization of and impact assessment for the aquatic systems of the Wyoming-Montana coal test area","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Terrell, T., 1978, Outline for the characterization of and impact assessment for the aquatic systems of the Wyoming-Montana coal test area.","costCenters":[],"links":[{"id":291949,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana;Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.98,40.99 ], [ -115.98,48.96 ], [ -104.05,48.96 ], [ -104.05,40.99 ], [ -115.98,40.99 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e9d8d4e4b008eaa4f3f67d","contributors":{"authors":[{"text":"Terrell, T.T.","contributorId":61871,"corporation":false,"usgs":true,"family":"Terrell","given":"T.T.","email":"","affiliations":[],"preferred":false,"id":497836,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25232,"text":"25232 - 1978 - Monitoring stress changes along active faults, southern California: semiannual technical report","interactions":[],"lastModifiedDate":"2014-07-15T11:12:58","indexId":"25232","displayToPublicDate":"1978-01-01T11:12:11","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Monitoring stress changes along active faults, southern California: semiannual technical report","docAbstract":"No abstract available.","language":"English","publisher":"Leighton and Associates","publisherLocation":"Irvine, CA","doi":"10.3133/25232","issn":"0364-7064","collaboration":"Sponsored by U.S. Geological Survey contract #14-08-0001-17735","usgsCitation":"Clark, B.R., 1978, Monitoring stress changes along active faults, southern California: semiannual technical report, ii, 14 p., https://doi.org/10.3133/25232.","productDescription":"ii, 14 p.","numberOfPages":"16","costCenters":[],"links":[{"id":290125,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64d9ee4b0001bd5147786","contributors":{"authors":[{"text":"Clark, Bruce R.","contributorId":18406,"corporation":false,"usgs":true,"family":"Clark","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":193336,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25293,"text":"25293 - 1978 - Marine sand and gravel mining","interactions":[],"lastModifiedDate":"2014-07-09T11:13:23","indexId":"25293","displayToPublicDate":"1978-01-01T11:12:10","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Marine sand and gravel mining","docAbstract":"No abstract available.","language":"English","publisher":"u.S. Geological Survey","doi":"10.3133/25293","issn":"0364-7064","usgsCitation":"Cruickshank, M., and Hess, H., 1978, Marine sand and gravel mining, 20 p., https://doi.org/10.3133/25293.","productDescription":"20 p.","numberOfPages":"20","costCenters":[],"links":[{"id":289622,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53be647ce4b0527d5d4097cb","contributors":{"authors":[{"text":"Cruickshank, M.J.","contributorId":16322,"corporation":false,"usgs":true,"family":"Cruickshank","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":193373,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, H.D.","contributorId":48484,"corporation":false,"usgs":true,"family":"Hess","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":193374,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70233073,"text":"70233073 - 1978 - Metamorphic forsterite and diopside from the ultramafic complex at the Tuolumne River, California","interactions":[],"lastModifiedDate":"2022-07-15T16:15:54.601721","indexId":"70233073","displayToPublicDate":"1978-01-01T11:04:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Metamorphic forsterite and diopside from the ultramafic complex at the Tuolumne River, California","docAbstract":"Metamorphic forsterite (Fo=98) and diopside (Wo:En:Fs=48.5:49.5:2.0) have been, formed from serpentinite within intensely sheared zones in the large ultramafic complex at the Tuolumne River near Sonora, Calif. Bladelike grains of forsterite are elongate, parallel to c, and have prominent idiomorphic faces developed in (010). Metamorphic diopside occurs as small grains, free of inclusions, in rocks containing forsterite. The formation of forsterite and forsterite +diopside in serpentinite probably took place by the following reactions:
antigorite+magnesite→2 forsterite+ fluid 3 antigorite+calcite→4 forsterite+diopside+fluid
Iron derived from the primary olivine and chromite has been oxidized almost entirely to magnetite and may be treated as an indifferent or accessory component. Stratigraphic reconstruction indicates that the total load pressures probably did not exceed 3 kilobars. At these pressures, the reaction should take place between 400° and 500°C with a fluid composition ranging from nearly pure H2O to less than 5 mole percent CO2. The restriction of forsterite and forsterite-f-diopside to shear zones may be attributed to the presence of carbonate in the rock prior to metamorphism and to the dilution of a CO2-bearing fluid phase by water coming from outside the area of the reaction.
","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Morgan, B., 1978, Metamorphic forsterite and diopside from the ultramafic complex at the Tuolumne River, California: Journal of Research of the U.S. Geological Survey, v. 6, no. 1, p. 73-80.","productDescription":"8 p.","startPage":"73","endPage":"80","costCenters":[],"links":[{"id":403822,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403819,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Tuolumne River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.75,\n 37.35\n ],\n [\n -119.85,\n 37.35\n ],\n [\n -119.85,\n 38.1\n ],\n [\n -120.75,\n 38.1\n ],\n [\n -120.75,\n 37.35\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Morgan, B. A.","contributorId":87128,"corporation":false,"usgs":true,"family":"Morgan","given":"B. A.","affiliations":[],"preferred":false,"id":846684,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70236555,"text":"70236555 - 1978 - Potential applications of satellite imagery in some types of natural resource inventories","interactions":[],"lastModifiedDate":"2022-09-09T17:05:58.96934","indexId":"70236555","displayToPublicDate":"1978-01-01T11:03:30","publicationYear":"1978","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"seriesNumber":"RM-55","title":"Potential applications of satellite imagery in some types of natural resource inventories","docAbstract":"Landsat satellite imagery has been routinely available to researchers and resource scientists since 1972. Many studies have demonstrated the application of Landsat imagery for conducting inventories and mapping various natural resources. Examples of applications presented in this paper include: timber volume
inventory, range productivity inventory, wildland vegetation mapping, inventory of rangeland conversion and irrigated lands, and mapping strip mine disturbance in forested areas. Costs and accuracies for each of these application areas are presented. Landsat data, used in its proper context with appropriate analysis techniques, supporting data, and sound sampling strategies, can be an effective tool in conducting natural resource inventories.
Other Landsat systems, scheduled for launch in 1978 and 1981, will provide continuity in the availability of Landsat data to users. Improvements in the quality and timeliness of data delivered to users, along with improved data handling procedures, analysis techniques, and improved sampling frameworks should increase the use of satellite imagery in natural resource inventories.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Integrated inventories of renewable natural resources: Proceedings of the workshop","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"conferenceTitle":"Integrated Inventories of Renewable Natural Resources","conferenceDate":"January 8-12, 1978","conferenceLocation":"Tucson, Arizona, United States","language":"English","publisher":"United States Department of Agriculture","usgsCitation":"Rohde, W.G., 1978, Potential applications of satellite imagery in some types of natural resource inventories, in Integrated inventories of renewable natural resources: Proceedings of the workshop, Tucson, Arizona, United States, January 8-12, 1978, p. 209-218.","productDescription":"10 p.","startPage":"209","endPage":"218","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":406469,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Lund, H. Gyde","contributorId":192744,"corporation":false,"usgs":false,"family":"Lund","given":"H.","email":"","middleInitial":"Gyde","affiliations":[],"preferred":false,"id":851387,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"LaBau, Vernon J.","contributorId":296391,"corporation":false,"usgs":false,"family":"LaBau","given":"Vernon","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":851388,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Ffolliott, Peter F.","contributorId":296392,"corporation":false,"usgs":false,"family":"Ffolliott","given":"Peter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":851389,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Robinson, David W.","contributorId":296393,"corporation":false,"usgs":false,"family":"Robinson","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":851390,"contributorType":{"id":2,"text":"Editors"},"rank":4}],"authors":[{"text":"Rohde, Wayne G.","contributorId":84630,"corporation":false,"usgs":true,"family":"Rohde","given":"Wayne","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":851384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70233069,"text":"70233069 - 1978 - Porphyry copper exploration model for northern Sonora, Mexico","interactions":[],"lastModifiedDate":"2022-07-15T16:02:22.246142","indexId":"70233069","displayToPublicDate":"1978-01-01T10:57:26","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Porphyry copper exploration model for northern Sonora, Mexico","docAbstract":"The regional tectonic pattern of the porphyry copper province of northern Sonora, Mexico, is similar to, but more complex than, the Colorado mineral belt. Four northeast-trending shear zones, spaced at 30- to 50-kilometer intervals from Hermosillo, Mexico, north to Nogales, Mexico, are interpreted from analysis of lineament data from Landsat-1 images. From comparison with other areas, these zones are believed to have Precambrian ancestry. North-northwest-trending lineaments, which commonly occur along range fronts, are interpreted to be the principal basin and range faults. North-south- and west-northwest-trending lineaments are believed to be related to lesser faults and fractures. Areas of hydrothermal alteration have been mapped on a regional scale by use of digital image-processing techniques. These altered areas occur on the flanks of the northeast-trending shear zones, generally near intersections with north-northwest-trending lineaments. This tectonic framework with associated alteration is similar to patterns in the Colorado Plateau, the porphyry copper province of Arizona, and central Mexico and is supported by relationships found in limited local mapping. The pattern of northeast-trending shear zones and north-northwest-trending faults in northern Sonora closely resembles the tectonic framework of the Colorado mineral belt. The younger sedimentary and volcanic cover, however, has not been eroded in Sonora as it has been in the Colorado mineral belt. This comparison with the Colorado mineral belt suggests that mineral deposits are most likely to be found in altered areas where a northeast-trending shear zone is intersected by north-northwest-trending faults. Seven areas with these characteristics have been defined in Sonora and are being evaluated by means of regional geophysical and geochemical data.
","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Raines, G.L., 1978, Porphyry copper exploration model for northern Sonora, Mexico: Journal of Research of the U.S. Geological Survey, v. 6, no. 1, p. 51-58.","productDescription":"8 p.","startPage":"51","endPage":"58","costCenters":[],"links":[{"id":403817,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403816,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Mexico","state":"Sonora","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.5,\n 29.5\n ],\n [\n -109,\n 29.5\n ],\n [\n -109,\n 31.5\n ],\n [\n -111.5,\n 31.5\n ],\n [\n -111.5,\n 29.5\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Raines, Gary L.","contributorId":48162,"corporation":false,"usgs":true,"family":"Raines","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":846683,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70233068,"text":"70233068 - 1978 - Hypothesis: Many earthquakes in the central and southeastern United States are causally related to mafic intrusive bodies","interactions":[],"lastModifiedDate":"2022-07-15T15:54:33.513593","indexId":"70233068","displayToPublicDate":"1978-01-01T10:49:54","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Hypothesis: Many earthquakes in the central and southeastern United States are causally related to mafic intrusive bodies","docAbstract":"Assessment of earthquake hazards in the United States is based largely upon knowledge acquired in the seismically active parts of the western United States. Earthquakes in the central and southeastern United States are seismologically and geologically very anomalous, however, compared with those in the western United States. For example, shallow earthquakes of magnitude 7-f in the western United States in general have tectonic surface faulting associated with them. No tectonic surface faulting, however, has been found to be associated with the New Madrid, Mo., earthquakes of 1811 and 1812, several of which had estimated magnitudes of 7-f. The lack of surface faulting is, in part, responsible for the fact that the New Madrid earthquakes have not been related with certainty to any particular geologic structural element, which makes assessment of the seismic hazards associated with possible similar future earthquakes very difficult. Geologic and seismologic data from the central and southeastern United States, however, suggest a spatial correlation between mafic intrusive rocks and seismic activity. An additional supportive correlation is that the trend of many dikes coincides with the trend of nodal planes in many fault-plane solutions. These correlations differ greatly from the direct correlation of earthquakes with faults in the western United States. Consideration of different concepts of earthquake sources in the central and southeastern. United States seems necessary- The preferred concept is that local high-stress concentrations, which may result in earthquakes, occur at or close to the contact of mafic intrusives and their felsic host rocks. Ancient rift zones may have been the primary control of the location of the mafic intrusives. Implications of a causal relation between mafic intrusives and seismicity are that more useful seismo-tectonic maps may be possible and that the source dimensions of the earthquakes would be small. Because of low attenuation, however, effects of earthquakes in the central and southeastern United States, even if relatively small because of smaller source dimensions, must be considered hazardous.
","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"McKeown, F.A., 1978, Hypothesis: Many earthquakes in the central and southeastern United States are causally related to mafic intrusive bodies: Journal of Research of the U.S. Geological Survey, v. 6, no. 1, p. 41-50.","productDescription":"10 p.","startPage":"41","endPage":"50","costCenters":[],"links":[{"id":403815,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403814,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94,\n 31\n ],\n [\n -76,\n 31\n ],\n [\n -76,\n 40\n ],\n [\n -94,\n 40\n ],\n [\n -94,\n 31\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McKeown, F. A.","contributorId":106100,"corporation":false,"usgs":true,"family":"McKeown","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":846682,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70233067,"text":"70233067 - 1978 - Accuracy and consistency comparisons of land use and land cover maps made from high-altitude photographs and Landsat multispectral imagery","interactions":[],"lastModifiedDate":"2022-07-15T15:48:51.544265","indexId":"70233067","displayToPublicDate":"1978-01-01T10:47:30","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Accuracy and consistency comparisons of land use and land cover maps made from high-altitude photographs and Landsat multispectral imagery","docAbstract":"Accuracy analyses for land use and land cover maps of the 74712-km2 Central Atlantic Regional Ecological Test Site were performed for a 1-percent sample of the area. Researchers compared Level II land use and land cover maps produced at three scales, 1:24000, 1:100000, and 1:250000 from high-altitude photographs, with point data obtained in the field. The same procedures were employed to determine the accuracy of the Level I land use and land cover produced at 1:250 000 scale from high-altitude photographs and color composite Landsat imagery.
The accuracy of the Level II maps was 85 percent at 1:24 000, 77 percent at 1:100 000, and 73 percent at 1:250 000. The accuracy of the Level I 1:250000 maps produced from high-altitude photographs was 77 percent and for those produced from Landsat multispectral imagery was 70 percent. The accuracy of the Level I land use maps produced using Landsat imagery is approximately that of the Level I land use maps produced from high-altitude photography with the exception of urban and built-up land. No built-up land was identified from Landsat imagery in the non-urban areas.
","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Fitzpatrick-Lins, K., 1978, Accuracy and consistency comparisons of land use and land cover maps made from high-altitude photographs and Landsat multispectral imagery: Journal of Research of the U.S. Geological Survey, v. 6, no. 1, p. 23-40.","productDescription":"18 p.","startPage":"23","endPage":"40","costCenters":[],"links":[{"id":403813,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403812,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Fitzpatrick-Lins, Katherine","contributorId":75906,"corporation":false,"usgs":true,"family":"Fitzpatrick-Lins","given":"Katherine","email":"","affiliations":[],"preferred":false,"id":846681,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70233062,"text":"70233062 - 1978 - Determination of runoff coefficients of storm-water-basin drainage areas on Long Island, New York, by using maximum-stage gages","interactions":[],"lastModifiedDate":"2022-07-15T15:43:18.632915","indexId":"70233062","displayToPublicDate":"1978-01-01T10:40:05","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Determination of runoff coefficients of storm-water-basin drainage areas on Long Island, New York, by using maximum-stage gages","docAbstract":"A method for determining runoff coefficients indirectly without direct measurement of volume of runoff was developed for drainage areas of selected storm-water basins on Long Island, N.Y., to expedite evaluation of basin performance. The method requires a maximum-stage gage to record the maximum water level attained in the basin during the storm, and a precipitation gage to record storm intensity at regular intervals. The maximum volume of runoff impounded in the basin during a storm is calculated from precipitation data, an arbitrarily estimated runoff coefficient, and the basin's dimensions and infiltration rate. The calculated result is then compared with the recorded maximum water level, and the process is repeated with increased or decreased coefficients on a trial basis until two of the resulting water-storage maxima closely bracket the recorded maximum. The runoff coefficient in effect during that storm is then interpolated or derived graphically from the calculated water-storage maxima. Results of data analyses suggest that a close approximation of a basin's infiltration rate may be used instead of a measured infiltration rate to calculate the runoff coefficient. Differences between measured and calculated runoff coefficients averaged less than 20 percent when based on average infiltration rates adjusted for water temperature and less than 10 percent when based on measured infiltration rates. Accuracy of the calculated runoff coefficient tends to decline as the interval between precipitation measurements increases. Precipitation data collected at 5- and 15-minute intervals gave accurate runoff coefficients regardless of storm duration, but data collected at 30- or 60-minute intervals gave widely varying results.
","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Aronson, D.A., 1978, Determination of runoff coefficients of storm-water-basin drainage areas on Long Island, New York, by using maximum-stage gages: Journal of Research of the U.S. Geological Survey, v. 6, no. 1, p. 11-21.","productDescription":"11 p.","startPage":"11","endPage":"21","costCenters":[],"links":[{"id":403811,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403810,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.102783203125,\n 40.40931350359072\n ],\n [\n -72.0428466796875,\n 40.40931350359072\n ],\n [\n -72.0428466796875,\n 41.236511201246216\n ],\n [\n -74.102783203125,\n 41.236511201246216\n ],\n [\n -74.102783203125,\n 40.40931350359072\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Aronson, D. A.","contributorId":20308,"corporation":false,"usgs":true,"family":"Aronson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":846680,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70098418,"text":"70098418 - 1978 - Cartographic research 1977","interactions":[],"lastModifiedDate":"2014-09-24T15:12:07","indexId":"70098418","displayToPublicDate":"1978-01-01T10:39:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Cartographic research 1977","docAbstract":"Two major subjects of the current research of the Topographic Division as reported here are related to policy decisions affecting the National Mapping Program of the Geological Survey. The adoption of a metric mapping policy has resulted in new cartographic products with associated changes in map design that require new looks in graphics and new equipment. The increasing use of digitized cartographic information has led to developments in data acquisition, processing, and storage and consequent changes in equipment and techniques.
\nThis report summarizes the activities in cartographic research and development for the 12-month period ending June 1977 and covers work done at the several facilities of the Topographic Division: the Western Mapping Center at Menlo Park, Calif., the Rocky Mountain Mapping Center at Denver, Colo., the Mid-Continent Mapping Center at Rolla, Mo., and the Eastern Mapping Center, the Special Mapping Center, the Office of Plans and Program Development, and the Office of Research and Technical Standards all at Reston, Va.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70098418","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Cartographic research 1977, vi, 73 p., https://doi.org/10.3133/70098418.","productDescription":"vi, 73 p.","numberOfPages":"80","costCenters":[{"id":587,"text":"Topographic Division","active":false,"usgs":true}],"links":[{"id":284150,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70098418.jpg"},{"id":286060,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70098418/report.pdf"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173.0,16.916667 ], [ 173.0,71.833333 ], [ -66.95,71.833333 ], [ -66.95,16.916667 ], [ 173.0,16.916667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53558ff9e4b0120853e8be73","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535638,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70119870,"text":"70119870 - 1978 - Comparative efficiencies of telemetry and visual techniques for studying ungulates, grouse, and raptors on energy development lands in southeastern Montana","interactions":[],"lastModifiedDate":"2014-08-11T10:35:18","indexId":"70119870","displayToPublicDate":"1978-01-01T10:32:57","publicationYear":"1978","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Comparative efficiencies of telemetry and visual techniques for studying ungulates, grouse, and raptors on energy development lands in southeastern Montana","docAbstract":"No abstract available.","largerWorkTitle":"Pecora IV symposium: Application of remote sensing data to wildlife management","conferenceTitle":"Pecora IV symposium","conferenceDate":"1978-01-01T00:00:00","conferenceLocation":"Sioux Falls, SD","language":"English","publisher":"National Wildlife Federation","publisherLocation":"Sioux Falls, SD","usgsCitation":"Biggins, E., and Pitcher, E., 1978, Comparative efficiencies of telemetry and visual techniques for studying ungulates, grouse, and raptors on energy development lands in southeastern Montana, 1 p.","productDescription":"1 p.","numberOfPages":"1","costCenters":[],"links":[{"id":291941,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.05,44.3582 ], [ -116.05,49.0014 ], [ -104.0396,49.0014 ], [ -104.0396,44.3582 ], [ -116.05,44.3582 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e9d8cde4b008eaa4f3f626","contributors":{"authors":[{"text":"Biggins, E.","contributorId":88303,"corporation":false,"usgs":true,"family":"Biggins","given":"E.","email":"","affiliations":[],"preferred":false,"id":497817,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pitcher, E.J.","contributorId":72312,"corporation":false,"usgs":true,"family":"Pitcher","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":497816,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70233060,"text":"70233060 - 1978 - Hydrochemistry and hydrodynamics of injecting an iron-rich pickling liquor into a dolomitic sandstone: A laboratory study","interactions":[],"lastModifiedDate":"2022-07-15T15:56:23.445751","indexId":"70233060","displayToPublicDate":"1978-01-01T10:32:49","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Hydrochemistry and hydrodynamics of injecting an iron-rich pickling liquor into a dolomitic sandstone: A laboratory study","docAbstract":"Waste pickling liquor containing high concentrations of iron salts was injected into cores of quartzite, sandstone, and dolomite in a laboratory study to determine what effect this procedure might have on the permeability of these rock types. Experiments were performed at field conditions 40°C and 13.8 MPa (megapascals) in a high-pressure triaxial chamber similar to that used in rock-mechanics testing but modified to allow downstream sample collection of effluent liquids and direct visual monitoring at in-situ conditions. Five samples were tested, ranging in effective porosity from 2.9 to 13 percent and in lithology from a quartzite to a dolomite. Hydraulic conductivity of the quartzitic samples remained unchanged during injection of over 50 pore volumes of pickling liquor, but significant decreases in the hydraulic conductivity of dolomitic samples were observed. Chemical analyses of effluents from a dolomitic sample suggest that carbonate minerals were dissolving and iron was precipitating. Clogging of pore space by CO2 entrapment or by CaCl2 precipitation did not seem to play a role in decreasing hydraulic conductivity because injection into a dolomitic core of more than 140 pore volumes of HCl at a concentration similar to that of the pickling liquor caused only a slight decrease in hydraulic conductivity compared with the decrease observed when an additional 30 pore volumes of pickling liquor were subsequently injected.
","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Ragone, S.E., Riley, F.S., and Dingman, R.J., 1978, Hydrochemistry and hydrodynamics of injecting an iron-rich pickling liquor into a dolomitic sandstone: A laboratory study: Journal of Research of the U.S. Geological Survey, v. 6, no. 1, p. 1-9.","productDescription":"9 p.","startPage":"1","endPage":"9","costCenters":[],"links":[{"id":403808,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403807,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ragone, Stephen E.","contributorId":74374,"corporation":false,"usgs":true,"family":"Ragone","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":846676,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Riley, Francis S.","contributorId":93028,"corporation":false,"usgs":true,"family":"Riley","given":"Francis","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":846677,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dingman, Robert James","contributorId":60190,"corporation":false,"usgs":true,"family":"Dingman","given":"Robert","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":846678,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}